Strike is a way of representing the 3D orientation of a planar surface on a 2D map. Fault can be characterized by brittle deformation in rocks. These faults can be oriented at any direction (Strike). Shear stresses can produce faults where movement can occur in strike direction.
Answer:
The statement that says 'on a geologic map, strike represents the directional orientation of a fault' is false.
Explanation:
